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THE INTERACTION BETWEEN ESTUARINE PL...

ZHANG, QINGHUA.

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THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA)./
作者:	ZHANG, QINGHUA.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 1985,
面頁冊數:	79 p.
附註:	Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.
Contained By:	Dissertation Abstracts International47-01B.
標題:	Physical oceanography. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=8529464

THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
ZHANG, QINGHUA.

THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA). - Ann Arbor : ProQuest Dissertations & Theses, 1985 - 79 p.

Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.

Thesis (Ph.D.)--North Carolina State University, 1985.

A simple analytical model is developed to describe the steady flow in an estuary-shelf interaction region where the water is treated as a two-layer density stratified flow. The motion is expanded in terms of the relative thickness of the Ekman layer, E(,v)(' 1/2). The order-zero flow is geostrophic in each layer. Balancing of order-one quantities reduces the system to two vorticity equations relating the pressure field with the displacement of the interface and the bottom topography. An explicit solution is obtained for the case of linear offshore sloping bottom. The flow behaviour of the river water plume depends on the vertical structure of the flow at the river mouth, the bottom topography and the ambient coastal flow. Under certain conditions, a salinity front exists as an offshore boundary of the river plume. These results are compared with observations for the Changjiang River (in China), and the Chesapeake Bay and Savannah River (in US) estuaries.Subjects--Topical Terms:

3168433
Physical oceanography.

THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
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245 1 4 $a THE INTERACTION BETWEEN ESTUARINE PLUMES AND CONTINENTAL SHELF WATERS (CHESAPEAKE BAY, GEORGIA, PEOPLE'S REPUBLIC OF CHINA).
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 1985
300 $a 79 p.
500 $a Source: Dissertation Abstracts International, Volume: 47-01, Section: B, page: 1200.
502 $a Thesis (Ph.D.)--North Carolina State University, 1985.
520 $a A simple analytical model is developed to describe the steady flow in an estuary-shelf interaction region where the water is treated as a two-layer density stratified flow. The motion is expanded in terms of the relative thickness of the Ekman layer, E(,v)(' 1/2). The order-zero flow is geostrophic in each layer. Balancing of order-one quantities reduces the system to two vorticity equations relating the pressure field with the displacement of the interface and the bottom topography. An explicit solution is obtained for the case of linear offshore sloping bottom. The flow behaviour of the river water plume depends on the vertical structure of the flow at the river mouth, the bottom topography and the ambient coastal flow. Under certain conditions, a salinity front exists as an offshore boundary of the river plume. These results are compared with observations for the Changjiang River (in China), and the Chesapeake Bay and Savannah River (in US) estuaries.
590 $a School code: 0155.
650 4 $a Physical oceanography. $3 3168433
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792 $a 1985
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=8529464